Structure of Mg30 explored via in-beam γ-ray spectroscopy

N. Kitamura et al.
Phys. Rev. C 102, 054318 – Published 12 November 2020

Abstract

Background: In the “island of inversion,” ground states of neutron-rich sd-shell nuclei exhibit strong admixtures of intruder configurations from the fp shell. The nucleus Mg30, located at the boundary of the island of inversion, serves as a cornerstone to track the structural evolution as one approaches this region.

Purpose: Spin-parity assignments for excited states in Mg30, especially negative-parity levels, have yet to be established. In the present work, the nuclear structure of Mg30 was investigated by in-beam γ-ray spectroscopy mainly focusing on firm spin-parity determinations.

Method: High-intensity rare-isotope beams of Mg31, Mg32, Si34, and P35 bombarded a Be target to induce nucleon removal reactions populating states in Mg30. γ rays were detected by the state-of-the-art γ-ray tracking array GRETINA. For the direct one-neutron removal reaction, final-state exclusive cross sections and parallel momentum distributions were deduced. Multinucleon removal reactions from different projectiles were exploited to gain complementary information.

Results: With the aid of the parallel momentum distributions, an updated level scheme with revised spin-parity assignments was constructed. Spectroscopic factors associated with each state were also deduced.

Conclusions: Results were confronted with large-scale shell-model calculations using two different effective interactions, showing excellent agreement with the present level scheme. However, a marked difference in the spectroscopic factors indicates that the full delineation of the transition into the island of inversion remains a challenge for theoretical models.

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  • Received 25 June 2020
  • Accepted 9 October 2020

DOI:https://doi.org/10.1103/PhysRevC.102.054318

©2020 American Physical Society

Physics Subject Headings (PhySH)

Nuclear Physics

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Vol. 102, Iss. 5 — November 2020

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